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Sierra Mono Museum

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Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Sierra Mono Museum
Phone:
+1 559-877-2115

Hours:
SundayClosed
MondayClosed
TuesdayClosed
Wednesday10am - 3pm
Thursday10am - 3pm
Friday10am - 3pm
Saturday10am - 3pm


The Sierra Nevada is a mountain range in the Western United States, between the Central Valley of California and the Great Basin. The vast majority of the range lies in the state of California, although the Carson Range spur lies primarily in Nevada. The Sierra Nevada is part of the American Cordillera, a chain of mountain ranges that consists of an almost continuous sequence of such ranges that form the western backbone of North America, Central America, South America and Antarctica. The Sierra runs 400 miles north-to-south, and is approximately 70 miles across east-to-west. Notable Sierra features include Lake Tahoe, the largest alpine lake in North America; Mount Whitney at 14,505 ft , the highest point in the contiguous United States; and Yosemite Valley, sculpted by glaciers from one-hundred-million-year-old granite. The Sierra is home to three national parks, twenty wilderness areas, and two national monuments. These areas include Yosemite, Sequoia, and Kings Canyon National Parks; and Devils Postpile National Monument. The character of the range is shaped by its geology and ecology. More than one hundred million years ago during the Nevadan orogeny, granite formed deep underground. The range started to uplift four million years ago, and erosion by glaciers exposed the granite and formed the light-colored mountains and cliffs that make up the range. The uplift caused a wide range of elevations and climates in the Sierra Nevada, which are reflected by the presence of five life zones . Uplift continues due to faulting caused by tectonic forces, creating spectacular fault block escarpments along the eastern edge of the southern Sierra. The Sierra Nevada has a significant history. The California Gold Rush occurred in the western foothills from 1848 through 1855. Due to inaccessibility, the range was not fully explored until 1912.
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From Wikipedia, the free encyclopedia.

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